Official Series Description


Lab Data Summary

Aggregate lab data for the FORT ROCK soil series. This aggregation is based on all pedons with a current taxon name of FORT ROCK, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to FORT ROCK were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
2395P005794OR037001Fort Rock6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4076138,-120.9913795

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FORT ROCK soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the FORT ROCK series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the FORT ROCK series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the FORT ROCK series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D mountains figure.

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Competing Series

Soil series competing with FORT ROCK share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the FORT ROCK series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the FORT ROCK series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with FORT ROCK, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

No block diagrams are available.

Map Units

Map units containing FORT ROCK as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Bonnick-Fort Rock complex, 0 to 2 percent slopes1711016722861t44qor62019921:24000
Fort Rock-Morehouse complex, 1 to 5 percent slopes3231276816898321tqdqor63520061:24000
Bonnick-Fort Rock complex, 0 to 2 percent slopes217928016897281tq9cor63520061:24000
Fort Rock-Suckerflat complex, 0 to 8 percent slopes325833516898341tqdsor63520061:24000
Bonnick-Fort Rock complex, 1 to 8 percent slopes218736816897291tq9dor63520061:24000
Fort Rock-Lapham complex, 0 to 2 percent slopes320551516898291tqdmor63520061:24000
Fort Rock ashy sandy loam, 0 to 2 percent slopes317409716898261tqdjor63520061:24000
Kunceider-Fort Rock complex, 1 to 5 percent slopes390335916898971tqgtor63520061:24000
Fort Rock-Bonnick complex, 0 to 2 percent slopes319301816898281tqdlor63520061:24000
Fort Rock-Morehouse complex, moist, 0 to 8 percent slopes324260916898331tqdror63520061:24000
Bonnick-Fort Rock complex, low precipitation, 1 to 8 percent slopes219231016897301tq9for63520061:24000
Fort Rock gravelly ashy sandy loam, 1 to 8 percent slopes318202116898271tqdkor63520061:24000
Cinderfall-Fort Rock-Kunceider complex, 1 to 8 percent slopes249197516897591tqbcor63520061:24000
Fort Rock-Morehouse complex, 0 to 2 percent slopes322165916898311tqdpor63520061:24000
Fort Rock-Lapham complex, warm, 0 to 10 percent slopes32196216898301tqdnor63520061:24000

Map of Series Extent

Approximate geographic distribution of the FORT ROCK soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .